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contributor authorArved J. Raudkivi
date accessioned2017-05-08T20:42:40Z
date available2017-05-08T20:42:40Z
date copyrightJanuary 1997
date issued1997
identifier other%28asce%290733-9429%281997%29123%3A1%2858%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/24335
description abstractSome 30 years ago, John F. Kennedy laid the foundations for the description of the geometry of sand waves on stream beds by the potential flow model. Since then, the analysis has been extensively refined and extended, but no rigorous description of the small features, called ripples, exists. The present study attempts a “stock-taking” of the data and the various behavioral concepts with the aim of encouraging researchers to improve our knowledge of the physics of features called ripples. Various trends are identified from the data. It is deduced that ripples act as roughness elements of the boundary. The ripple troughs are “filled” with the energy-consuming lee vortices. The main flow is over the ripple crests and lee vortices and does not interact with the bed geometry. The “roughness layer” of ripples and vortices is within the constant shear layer and is affected by the flow depth only as far as it affects the velocity distribution and alters the shear stress on the bed.
publisherAmerican Society of Civil Engineers
titleRipples on Stream Bed
typeJournal Paper
journal volume123
journal issue1
journal titleJournal of Hydraulic Engineering
identifier doi10.1061/(ASCE)0733-9429(1997)123:1(58)
treeJournal of Hydraulic Engineering:;1997:;Volume ( 123 ):;issue: 001
contenttypeFulltext


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